Seismological Research Letters; September/October 2006; v. 77; no. 5;
p. 532-543; DOI: 10.1785/gssrl.77.5.532
© 2006 Seismological Society of America
The Current State of Seismic Monitoring in Puerto Rico
John F. Clinton1,3,
Georgia Cua1,3,
Víctor Huérfano2,
Christa G. von Hillebrandt-Andrade2, and
José Martínez Cruzado1
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The U.S. Commonwealth of Puerto Rico has a population of 3.8 million (2000
Census), a higher population density than any U.S. state. The island,
approximately 160 km east to west by 50 km north to south, is bounded by
offshore active faults on all sides. Numerous local and regional events in the
recorded history with M > 7.0, some of which have generated tsunamis, have
caused extensive damage to local infrastructure, though the last significant
ground motions were felt onshore in 1918. The U.S. Geological Survey hazard
maps (Mueller et al.
2003) indicate that the seismic hazard is similar to the Basin and
Range province in the Western United States, and the island is assigned
Seismic Zone 3 in the current standard building code in Puerto Rico, the 1997
UBC. The significant hazard, combined with the large population and untested
infrastructure, results in a potentially devastating combination for Puerto
Rico. Efficient emergency response in the event of a large earthquake will be
crucial to minimizing the resultant loss of human life and disruption of
lifeline systems. The first step in providing an appropriate response to such
a disaster is a timely knowledge of the magnitude, location, and expected
ground shaking and damage patterns from a large earthquake. This requires a
modern and dense seismic network, capable of not only recording the earthquake
ground motion without saturation but also doing so in real time and then
providing data for near-immediate analysis that can be made available to
emergency services and the community at large.
The seismicity of the island, as well as the northeastern Caribbean region
in general (including the U.S. and British Virgin Islands), is monitored
jointly by the Puerto Rico Seismic Network (PRSN) and the Puerto Rico Strong
Motion Program (PRSMP), both operating within the University of . . . [Full Text of this Article]
Puerto Rico Strong Motion Program (PRSMP)
Department of Civil
Engineering
University of Puerto Rico at Mayagüez,
Mayagüez,
PR
martinez@uprm.edu
(J.
M.C.)
Puerto Rico Seismic Network (PRSN)
Geology Department
University of Puerto Rico at Mayagüez,
Mayagüez,
PR
victor@midas.uprm.edu
(V.H.)
christa@midas.uprm.edu
(C.H.A.)
Swiss Seismological Service (SED)
Institute of Geophysics
Swiss Federal Institute of Technology (ETH)
Zurich,
Switzerland
jclinton@sed.ethz.ch,georgia.cua@sed.ethz.ch
(J.C., G. C.)
1 Puerto Rico Strong Motion Program, Department of Civil Engineering and
Surveying, University of Puerto Rico at Mayagüez
2 Puerto Rico Seismic Network, Geology Department, University of Puerto Rico at
Mayagüez
3 Now at Swiss Seismological Service (SED), Institute of Geophysics, ETH
Hönggerberg, Switzerland
Copyright © 2009 by Seismological Society of America